. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography — 40°30 H. Figure Above: Total suspended load in mg/liter, at 10 meters depth, November 1973. Below: Generalized circulation pattern of the New York Bight apex as inferred, from the distribution of suspended sediments during fall3 1973. Dashed, line is mean position of boundary between more turbid coastal water and less turbid offshore water. Turbid, brackish surface effluent of harbor flows down New Jersey shore. Clockwise gyre is driven by s
. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography — 40°30 H. Figure Above: Total suspended load in mg/liter, at 10 meters depth, November 1973. Below: Generalized circulation pattern of the New York Bight apex as inferred, from the distribution of suspended sediments during fall3 1973. Dashed, line is mean position of boundary between more turbid coastal water and less turbid offshore water. Turbid, brackish surface effluent of harbor flows down New Jersey shore. Clockwise gyre is driven by southwesterly drift of offshore shelf water and, on bottom, by the influx of saline water into the harbor. Solid arrows are currents that appear to be persistent. 78. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Atlantic Oceanographic and Meteorological Laboratories; Pacific Oceanographic Laboratories; United States. Environmental Science Services Administration. Research Laboratories; Environmental Research Laboratories (U. S. ). Washington, D. C. : U. S. Dept. of Commerce, Environmental Science Services Administration, Research Laboratories : For sale by Supt. of Docs. U. S. G. P. O.
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